The flow of time in the Connecticut valley : $b geological imprints — John Shaqi
The flow of time in the Connecticut valley : $b geological imprintsBain, George W. (George William)
Science
The flow of time in the Connecticut valley : $b geological imprints
Bain, George W. (George William)
Geology -- Connecticut River Valley
Devil or no devil, those huge columns had a hot origin. The dark rock in
them is part of the main lava sheet which stretches across the valley in
the Holyoke Range and swings southward in the Nonotuck—Mount Tom Range.
The lava poured out of a series of volcanoes which were strung out along
a fissure about three miles to the east, and the molten mass had a
temperature of 1200° to 1300° C. The hot lava radiated its heat to the
sandstone below and to the air above; and, as it cooled, it contracted
like any other substance. The shrinkage was so great that series of
cracks formed in regular pattern, with each crack perpendicular to the
cooling surface. The stresses producing the fissures were equal in all
directions and would have made circular cracks and cylindrical columns;
but cylinders have non-cylindrical spaces between them, and the pattern
in which the columns are most nearly cylindrical and yet completely
occupy all space is hexagonal. So contraction broke the lava into
hexagonal columns perpendicular to the cooling surface. The columns are
parallel where the lava floor is regular but are curved or radial where
the floor is rolling.
Pl. 8. _Trap ridges, near and far._
[Illustration: a. _View of Titan’s Piazza at Hockanum showing the
columns resting upon the gently inclined sandstone._]
[Illustration: b. _View of the Springfield lowland from the
Westfield marble quarry. The Wilbraham Mts. appear in the distance.
The trap ridge extends through the middle and is breached by the
Westfield River._]
The columns on Titan’s Pier lie across the river from the
Northampton-Holyoke road in the narrow gap at Mount Tom station. The
basalt flow is inclined 15° southeastward, and the columns stand
perpendicular to the surface—hence they are inclined with respect to the
water level. Doubtless the devil docked his boat on the gently inclined
rock surface of the cove on the downstream side of the pier.
Titan’s Piazza is situated east of the road to the Mount Holyoke House.
It is an extremely narrow ledge backed by a stockade of columns. The
front of the piazza is literally strewn with wreckage from the house,
for a slope over 100 feet high is covered with angular pieces of basalt
which have fallen from the back wall. The lower ends of the columns
break off into shallow hexagonal saucers with the concave sides up. Many
have slid down the slope, to the delight of the birds that bathe in
them. Higher up the cliff, the saucers become deeper, and towards the
top the columns scale on into bullet shaped masses.
_Westfield Marble Quarry_
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account